Kirkiite is a rare lead-bismuth sulfosalt typically found as microscopic grains or small aggregates within hydrothermal ore deposits. It is best identified through lab analysis or X-ray diffraction, as it is macroscopically indistinguishable from other lead-gray sulfide minerals found in similar geologic settings.

Hardness
3.5
Mohs
Luster
Metallic
Streak
Black
Transparency
Opaque

Is this kirkiite?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch kirkiite with a known reference. Kirkiite sits at Mohs 3.5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: black.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: metallic.
  • 4
    Match the color range
    Compare against the expected color range: tin white.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: microscopic crystals, pseudo hexagonal, twinning common.

Often confused with

Kirkiite vs. its common look-alikes, and how to tell them apart in the field.

Often found alongside kirkiite

Minerals reported to co-occur with kirkiite. Spotting these in float or country rock is a strong cue you are in the right ground.

All properties

Chemical formula
Pb₁₀Bi₃As₃S₁₉
Mohs hardness
3.5
Density
6.80 g/cm³
Colors
Streak
Black
Luster
Metallic
Transparency
Opaque
Crystal system
Monoclinic
Crystal habit
Microscopic crystals, pseudo hexagonal, twinning common
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
In a hydrothermal Pb-Zn deposit (Kirki, Greece); in a volcanic fumarole, formed at about 470 °C (Vulcano, Italy)

Where rockhounds find kirkiite

Classic worldwide localities

  • Aghios Philippos Pb-Zn deposit, near Kirki, Thrace, Greece (type locality)
  • La Fossa crater, Vulcano, Lipari Islands, Italy

Field-hunting tip

Where it forms: In a hydrothermal Pb-Zn deposit (Kirki, Greece); in a volcanic fumarole, formed at about 470 °C (Vulcano, Italy). If you start seeing cosalite, bismuthinite, bismuthian jordanite in float, you are in the right ground. Typical habit: microscopic crystals, pseudo hexagonal, twinning common. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify kirkiite?+
Mohs hardness is 3.5. Luster: metallic. The streak is black. Common colors include tin white.
Where is kirkiite found?+
Notable localities include Aghios Philippos Pb-Zn deposit, near Kirki, Thrace, Greece (type locality); La Fossa crater, Vulcano, Lipari Islands, Italy.
Is kirkiite safe to handle?+
Kirkiite contains arsenic and lead and calls for real care. Contains lead and bismuth; handle with care and wash hands after contact. Avoid inhaling dust or powder.
What rocks look like kirkiite?+
Kirkiite is most often confused with Galena, Cosalite, Kobellite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with kirkiite?+
Kirkiite commonly co-occurs with Cosalite, Bismuthinite, Bismuthian jordanite, Seligmannite, Levyclaudite, Sphalerite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does kirkiite form in?+
Where it forms: In a hydrothermal Pb-Zn deposit (Kirki, Greece); in a volcanic fumarole, formed at about 470 °C (Vulcano, Italy). Working float back to the host body is the standard way to chase a fresh occurrence.
What is kirkiite used for?+
Kirkiite is used in collector.

Find kirkiite on the map

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